Determining Mineral Composition in the Ultraviolet Spectral Region from 200 to 400 Nanometres

Details Determining Mineral Composition in the Ultraviolet Spectral Region from 200 to 400 Nanometres Determining Mineral Composition in the Ultraviolet Spectral Region from 200 to 400 Nanometres

Mar 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006lpi....37.2158m&link_type=abstract

37th Annual Lunar and Planetary Science Conference, March 13-17, 2006, League City, Texas, abstract no.2158

Physics

Scientific paper

Ultraviolet (200-400 nm) reflectance spectra of major rock-forming
minerals (e.g., olivine, pyroxene, plagioclase feldspar, ilmenite)
exhibit measurable differences in their spectral properties. This
suggests that these minerals can be discriminated in the UV.

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